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Autores principales: Kuhn, Gerhard, Hillenbrand, Claus-Dieter, Kasten, Sabine, Smith, James A, Nitsche, Frank-Oliver, Frederichs, Thomas, Wiers, Steffen, Ehrmann, Werner, Klages, Johann Philipp, Mogollón, José M
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2017
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Acceso en línea:https://doi.org/10.1594/PANGAEA.873755
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author Kuhn, Gerhard
Hillenbrand, Claus-Dieter
Kasten, Sabine
Smith, James A
Nitsche, Frank-Oliver
Frederichs, Thomas
Wiers, Steffen
Ehrmann, Werner
Klages, Johann Philipp
Mogollón, José M
author_facet Kuhn, Gerhard
Hillenbrand, Claus-Dieter
Kasten, Sabine
Smith, James A
Nitsche, Frank-Oliver
Frederichs, Thomas
Wiers, Steffen
Ehrmann, Werner
Klages, Johann Philipp
Mogollón, José M
collection Datos científicos de ciencias marinas y ambientales
contents Subglacial lakes are widespread beneath the Antarctic ice sheet but their control on ice sheet dynamics and their ability to harbour life remain poorly characterised. Here we present the evidence for a palaeo-subglacial lake on the Antarctic continental shelf. A distinct sediment facies recovered from a bedrock basin in Pine Island Bay indicates deposition within a low-energy lake environment. Diffusive-advection modelling demonstrates that low chloride concentrations in the sediment pore water can only be explained by initial deposition of this facies in a freshwater setting. These observations indicate that an active subglacial meltwater network, similar to that observed beneath the extant ice sheet, was also active during the last glacial period. It also provides a new framework for refining exploration of these unique environments.
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institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle Sediment facies of a paleo-subglacial lake on the Antarctic continentral shelf
Kuhn, Gerhard
Hillenbrand, Claus-Dieter
Kasten, Sabine
Smith, James A
Nitsche, Frank-Oliver
Frederichs, Thomas
Wiers, Steffen
Ehrmann, Werner
Klages, Johann Philipp
Mogollón, José M
AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
Subglacial lakes are widespread beneath the Antarctic ice sheet but their control on ice sheet dynamics and their ability to harbour life remain poorly characterised. Here we present the evidence for a palaeo-subglacial lake on the Antarctic continental shelf. A distinct sediment facies recovered from a bedrock basin in Pine Island Bay indicates deposition within a low-energy lake environment. Diffusive-advection modelling demonstrates that low chloride concentrations in the sediment pore water can only be explained by initial deposition of this facies in a freshwater setting. These observations indicate that an active subglacial meltwater network, similar to that observed beneath the extant ice sheet, was also active during the last glacial period. It also provides a new framework for refining exploration of these unique environments.
title Sediment facies of a paleo-subglacial lake on the Antarctic continentral shelf
topic AWI_Paleo; Paleoenvironmental Reconstructions from Marine Sediments @ AWI
url https://doi.org/10.1594/PANGAEA.873755